Publication | Closed Access

The Upper Aptian to Lower Albian syn-rift carbonate succession of the southern Maestrat Basin (Spain): Facies architecture and fault-controlled stratabound dolostones

Rift SystemMarine GeologyEngineeringGeomorphologyGeographyQuaternary Tectonic DeformationGeologyUpper AptianRegional TectonicsGeochronologyNeotectonicsSouthern Maestrat BasinEarth ScienceRegional GeologyFault-controlled Stratabound DolostonesTectonics